西藏拉萨地体冈底斯岩基紫苏花岗岩中的
高密度C02包裹体成因及其地质意义*
沈昆1**,张泽明2.3, Santosh M4 ,董听2
Origin and geological significance of high-density CO2 fluid
inclusions in Charnockites from the Gangdese batholith,
Lhasa terrane,southern Tibet
Shen Kun1,Zhang Ze-Ming 2,3,Santosh M4,Dong Xin2
南京大学学报(自然科学版)
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2012, (3): 278
-294
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